Add to ORKGThe following descriptions of a 24-hour cycle of the flows of radiant energy in November 1974 were written as follow-up assignments to a class exercise measuring these energy flows at the Field Station (Meteorology 511 - Dynamic Meteorology I: Radiation). All the flows of short-wave (or solar) radiation (wave length less than 3 micrometers) and long-wave radiation (wave lengths 3 to 50 micrometers) were measured, and their interrelations calculated
Under the supervision of Professors Timothy Shedd, Sanford Klein, and William Beckman; 101pp.Solar r...
Solar radiation received at the Earth's surface (R-s) is comprised of two components, the direct rad...
Hourly Wangara boundary layer data (Clark et al., 1971) was used to substantiate previously derived ...
The following descriptions of a 24-hour cycle of the flows of radiant energy in November 1974 were w...
As with others of the numerous physical factors forming the nonliving environment of terrestrial eco...
The following descriptions of a 24-hour cycle of the flows of radiant energy in November 1974 were w...
The characteristics of solar energy arriving at the surface of the Earth are defined and the history...
24th annual AGU hydrology days was held at Colorado State University on March 10-12, 2004.Includes b...
During the past decade important advances have been made in the measurement of light and radiant ene...
Energy Balance Bowen Ratio System--Estimates of surface energy fluxes are a primary product of the d...
The radiation climate of Cache Valley was established f rom the continuous recordings of global and ...
Atmospheric radiation is the primary variable in nocturnal cooling, although wind has greater influ...
The paper presents a relationship between the relative sunshine duration and solar irradiation on th...
Measurements of total solar radiation were made on 7 March 1977. The sky was cloudless but a cooling...
Paper copies in Archives, Acc #:2013-0059Solar and net radiation received at Palmer, Alaska (61 ° 3 ...
Under the supervision of Professors Timothy Shedd, Sanford Klein, and William Beckman; 101pp.Solar r...
Solar radiation received at the Earth's surface (R-s) is comprised of two components, the direct rad...
Hourly Wangara boundary layer data (Clark et al., 1971) was used to substantiate previously derived ...
The following descriptions of a 24-hour cycle of the flows of radiant energy in November 1974 were w...
As with others of the numerous physical factors forming the nonliving environment of terrestrial eco...
The following descriptions of a 24-hour cycle of the flows of radiant energy in November 1974 were w...
The characteristics of solar energy arriving at the surface of the Earth are defined and the history...
24th annual AGU hydrology days was held at Colorado State University on March 10-12, 2004.Includes b...
During the past decade important advances have been made in the measurement of light and radiant ene...
Energy Balance Bowen Ratio System--Estimates of surface energy fluxes are a primary product of the d...
The radiation climate of Cache Valley was established f rom the continuous recordings of global and ...
Atmospheric radiation is the primary variable in nocturnal cooling, although wind has greater influ...
The paper presents a relationship between the relative sunshine duration and solar irradiation on th...
Measurements of total solar radiation were made on 7 March 1977. The sky was cloudless but a cooling...
Paper copies in Archives, Acc #:2013-0059Solar and net radiation received at Palmer, Alaska (61 ° 3 ...
Under the supervision of Professors Timothy Shedd, Sanford Klein, and William Beckman; 101pp.Solar r...
Solar radiation received at the Earth's surface (R-s) is comprised of two components, the direct rad...
Hourly Wangara boundary layer data (Clark et al., 1971) was used to substantiate previously derived ...